Deep water circulation in the Arabian Sea during the last glacial cycle: Implications for paleo-redox condition, carbon sink and atmospheric CO2 variability-Reference-Cited by-同舟云学术

Deep water circulation in the Arabian Sea during the last glacial cycle: Implications for paleo-redox condition, carbon sink and atmospheric CO2 variability

Published:2021-04 Issue: Volume:257 Page:106853
ISSN:0277-3791
Container-title:Quaternary Science Reviews
language:en
Short-container-title:Quaternary Science Reviews

Author:

Lathika N.^ORCID,Rahaman Waliur^ORCID,Tarique Mohd,Gandhi Naveen,Kumar Avinash,Thamban Meloth

Funder

Ministry of Earth Sciences

Publisher

Elsevier BV

Subject

Geology,Archeology,Archeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference110 articles.

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4. Glacial to Holocene changes in the surface and deep waters of the northeast Indian Ocean;Ahmad;Mar. Geol.,2012

5. Neodymium concentration and isotopic composition distributions in the southwestern Indian Ocean and the Indian sector of the Southern Ocean;Amakawa;Chem. Geol.,2019

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3. Global oceanic oxygenation controlled by the Southern Ocean through the last deglaciation;Science Advances;2024-01-19

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